LETTERS
TO THE
EDITOR
611
density was highest in LiF crystals through which the
debris
cleavage crack progressed most slowly.
surfaces, it has not been possible to measure their rate
that the dislocations play an important by
introduced
This suggests
during cleavage may
role in the ductility.
ductile
after immersion
in hot 20%
H&30,
followed by a water rinse. Sodium chloride is ductile after surface dissolution with water, after a dip into a dry ether solution
of stearic
acid,
of surface cracking
irregularities
on freshly
by the silver deposition
Also, reliable data on rate of ductility
It was also found that the ductility can be restored a variety of surface treatments. Brittle MgO
becomes
and surface
and after the
vacuum deposition of a layer of sodium chloride or gold. Some of these treatments are of such nature
cleaved method.
change on water
polished crystals are not yet available. Thus, direct correlations are not permitted. Since it is known that a small tensile stress accelerated
the rate of cracking
on water polished crystals, it is possible that a sufficient number of cracks may form rapidly under the influence
of stress induced
by
cleavage
and cause
freshly cleaved crystals rapidly to lose their ductility.
as to suggest that it is not always necessary to remove
X-ray surface damage detectable by electron diffraction also has been found(g) to occur more rapidly on
the surface layers to restore ductility. of restoration varies with the treatment;
tion of or reaction with atmospheric
sulfuric
acid treated
The extent for example,
MgO is not as ductile
freshly cleaved crystal.
as the
On the other hand, the stearic
acid solution renders NaCl more ductile than does the water treatment, which in itself results in greater ductility
than fresh cleavage.
Another
important
but as yet unexplained
result
is that the elastic modulus is also changed by surface treatment. If the ductility is improved, the modulus is decreased. For extent of reduction
cleavage faces than on water treated faces.
Adsorp-
gases could also
result in an increase in the surface strain and thus accelerate
cracking.
Finally,
it is also possible
cracks in a range of sizes below that detectable technique
that
by our
are formed rapidly after cleavage or other
surface treatment. It is obvious that further careful experimentation is
needed
ductility
before
the
basic
in these materials
processes
controlling
can be clearly
sulfuric acid treated MgO, the varies with the time of exposme
defined.
R. A. LAD C. A. STEARNS
to the acid. Reductions in modulus as much as 50 per cent of the original value have been obtained. The
M.
G. DEL DUCA
stress-strain curves reported for NaCl by Aerts and Dekeyser”’ also appear to show a variation in the
National Advisory Committee for Aeronautics
elastic region with various specimen treatments. experiments have been reported(7t8) Recently,
Cleveland, Ohio
which give evidence that the atmosphere
1. A. A. GRIFFITH,Phil Trans. Roy. SW. A221, 163 (1920); Proc. Intern. Congr. App. Me&. (Delft), 55 (1924). 2. A. JOFFE, The Physics cf Crystals. McGraw-Hill, New York (1928). 3. R. A. LAD, J. A&. Phys. 93, 800 (1952). 4. F. I. METZ and R. A. LAD, J. Phys. Chem. 60, 277 (1956). 5. J. E. LENNARD-JONESand B. M. DENT, Proc. Roy. Sot. Lond. 121, 247 (1928). 6. J. J. GILMAN, J. Metals (Tmnmctions) 9, 449 (1957). 7. E. AERTS and W. DEKEYSER, Acta Met. 4, 557 (1956). 8. A. E. GORUM. E. R. PARKER and J. A. PASK. Paoer presented at American Ceramic Society Meeting ai Alfred University, Alfred, N.Y. (Sept. 9-10, 1957). 9. H. LEIDER, Phys. Rev. 101,56 (1956).
crystals
are stored after cleavage
in which the
has an importatit
bearing on the retention of ductility. Crystals of NaCl were found to remain ductile in vacuum or helium or if stored under oil.
They rapidly
become
brittle
if
exposed to gaseous nitrogen or oxygen. The
low
rate
temperature
of microcrack
formation
and the atmospheric
at room
effects on ductility
raise questions regarding the adequacy
of the original
postulate that the presence of microcracks
is the main
cause for the brittle behavior of ionic crystals. The data may be taken to indicate that ductility is restricted
by
additional
mechanisms.
with atmospheric
gases.
It is possible, however, that the limited body of information available at present could still be interpreted in terms of microcracks. The rate of cracking was measured in water polished crystals, whereas the relatively rapid reduction measured on freshly cleaved
Laboratory References
Received February 10, 1958.
One of these
might be, for example, the restriction of dislocation motion by the presence of surface layers formed by interaction
Lewis Flight Prop&on
in ductility has been crystals. Because of
Dilatational
strain due to dislocations in copper
Clarebrough, Hargreaves, and West(l) have recently measured both the stored energy and the macroscopic density changes in some specimens of plastically deformed copper. They have interpreted the density changes in terms of densities of dislocations by using a calculation of Stehle and Seeger.t2) The latter
ACTA
612
authors
have
calculated
the
with a screw dislocation
METALLURGICA,
dilatation
also used Cottrell’s(3) calculation from
their
of the elastic energy
energy
measurements.
densities The
dis-
location densities found in this way agree with those derived from the dilatational effects. The purpose of the
present
observed
communication
relationship
is to
between
energy can be obtained dynamic
arguments,
1958
associated
to estimate the dislocation
stored
6,
(5)
in copper on the basis of a
detailed model of the atomic interactions in the vicinity of the dislocation. Clarebrough et aZ.(l) have of a dislocation
VOL.
show
dilatation
approximately
without
that
the
where @ is the isothermal compressibility. We will apply (5) to th e present problem, interpreting E as the shear strain energy of a dislocation, and taking (a In ,u/&)~
from the work of Lazarus.c4)
TABLE 1. Summary of the results of Lazarus Elastic constant
Value (dyn/cm?
and stored
from thermo-
reference to an atomic
(~@h#/\
7.56 x 10” 2.36 x 10”
&(C,;%,,)
(3 In IJ/%)F (cms/cal)
n
0.11 x lo-” 0.23 x 10-l’
~
for copper. B
0.17 x 10-4 0.67 x lo-”
~
model of a dislocation. The results of Lazarus for copper are summarized
The elastic continuum model of a dislocation, which was used by Cottrell,(3) will also be used here.
in Table
In this model the elastic energy of a dislocation
dynamic arguments assume an isotropic solid, whereas
to a pure shear strain in the crystal. origin of the dilatational dislocation
The qualitative
strain associated
is then as follows:
is due
with the
It has been shown by
Lazarust4) that the elastic shear modulus of a crystal is changed by dilatation
of the latter.
energy of a crystal subjected
Therefore the
to an elastic shear strain
can be lowered by changing the volume of the crystal in such a way as to lower the shear modulus. In order to describe thermodynamic
this effect by a quantitative
relation, we consider a system which
was analyzed by Zenerc5) in another connection, namely, a cylindrical specimen of radius R and length L, subjected
to a torque
and to a hydrostatic entire
surface.
r applied at the two ends,
pressure
The
specimen
2, applied
d(E+pV-
TS)=
to
where E is the energy of the specimen,
V is its volume
and S its entropy, and 4 is the angle of twist. (I) is a perfect differential, the relation
Since
Following
Zener,
work done by the torque
we denote
in twisting
by
E the
the specimen
from equilibrium to 4 at constant pressure temperature, and divide both sides of (2) by r:
and
for r the formula of elastic theory i?pRi r=2L-
4
of copper, the exact value of (a In &n),
which
It seems likely
that most of the shear will be of the type
requires
the least energy,
namely,
that
which the shear modulus is lowest. Since $(C,, is less than one-third +(C,, -
C,,)
for C,,)
as great as C,,, the figures for
will be used in comparing equation (5)
with the experiments. TABLE 2. Comparison of the observed dilatation”’ with that calculated from equation (5), using the pressure dependence of &(C,, - Cl,). o/0Deformation
Stored energy (cal/cm5)
AVIV Calculated
AVIV Observed
0.57 x 10-a 0.76 x lo-” 0.88 x 10-e
0.91 x 10-4 1.38 x 1O-4 1.93 x IO-”
/ 30
0.85 1.14 1.31
::
~
~
The comparison is given in Table 2. It is seen that the calculated dilatations are too small by roughly a factor
two.
In view
of a dislocation
of the fact can only
that
any elastic
be approximate,
because much of the energy is stored in regions where the strain is far beyond the elastic limit, this agreement is as good as can be expected. Xemiconductor and Solid State
R. W. KEYES
Physics Department Westinghowe Research Laboratories Pittsburgh 35, Penn.
(3) Substituting
however,
theory
(2) is satisfied.
properties
be
(1)
model and our thermo-
to be used in (5) is not apparent.
for this system
Vdp+rdf$-#ST
Since Cottrell’s
two shear moduli are required to describe the elastic
over the
is considered
elastically isotropic. Zener derives the perfect differential form
1.
(4)
References 1. L. M. CLAREBROUOH, M. E. HARGREAVES and G. W. WEST, Acta Met. 5, 738 (1957). 2. H. STEELEand A. SEEGER,2. Phys. 148, 217 (1956). 3. A. H. COTTRELL,Dislocations and Plastic Flow in Crystals. Clarendon Press, Oxford (1953). 4. D. LAZARUS,Phys. Rev. 76, 545 (1949). 5. C. ZENER, Acta Cryst. 2, 163 (1949). Received February 14, 1958.